Metabarcoding Insights Into the Trophic Behavior and Identity of Intertidal Benthic Foraminifera
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Endosymbiont-Bleaching in Epiphytic Populations of Sorites Dominicensis
SYMBIOSIS (2006) 42, xx–xx ©2006 Balaban, Philadelphia/Rehovot ISSN 0334-5114 Endosymbiont-bleaching in epiphytic populations of Sorites dominicensis Susan L. Richardson Wilkes Honors College, Florida Atlantic University, 5353 Parkside Drive, Jupiter, FL, 33458; and Department of Paleobiology, National Museum of Natural History, Washington, DC 20560, USA, Tel. +1-561-799-8604, Fax. +1-561-799-8602. Email. [email protected] (Received July 20, 2006; Accepted September 26, 2006) Abstract Episodes of symbiont-bleaching have been documented in field studies of epiphytic populations of the dinoflagellate- bearing foraminiferan Sorites dominicensis from Jupiter Sound in the Indian River Lagoon, Florida, and Carrie Bow Cay and Twin Cays, Belize. In August 2003, 13–16% of the population in Jupiter Sound exhibited evidence of bleaching, with cytoplasm that was either mottled or totally white. In July 2005, 18% of the population on the reef flat off Carrie Bow Cay, and 4% of the population in the tannin-stained waters of Boston Bay, Twin Cays, exhibited signs of bleaching. Symbiont bleaching in soritid foraminiferans may be a more widespread and recurrent phenomenon than has previously been recognized. Bleaching appears to be triggered by a combination of environmental factors that are similar to the conditions that trigger bleaching in corals, such as: subaerial exposure during extreme low spring tides in the summer months, high water temperatures, increased irradiance, exposure to light in the ultraviolet or blue light spectra, and periodic disturbance by hurricanes. The endosymbionts in S. dominicensis, and other soritid foraminiferans, are members of the Symbiodinium clade of dinoflagellates that comprise the zooxanthellae in cnidarians and molluscs, thus this foraminiferal host-symbiont system has potential utility as a model system for the experimental study of the cellular and molecular mechanisms underlying coral bleaching. -
Recent Benthic Foraminifera from the Itaipu Lagoon, Rio De Janeiro (Southeastern Brazil)
12 5 1959 the journal of biodiversity data 15 September 2016 Check List LISTS OF SPECIES Check List 12(5): 1959, 15 September 2016 doi: http://dx.doi.org/10.15560/12.5.1959 ISSN 1809-127X © 2016 Check List and Authors Recent benthic foraminifera from the Itaipu Lagoon, Rio de Janeiro (southeastern Brazil) Débora Raposo1*, Vanessa Laut2, Iara Clemente3, Virginia Martins3, Fabrizio Frontalini4, Frederico Silva5, Maria Lúcia Lorini6, Rafael Fortes6 and Lazaro Laut1 1 Laboratório de Micropaleontologia (LabMicro), Universidade Federal do Estado do Rio de Janeiro – UNIRIO. Avenida Pasteur 458, Urca, Rio de Janeiro, CEP 22290-240, RJ, Brazil 2 Universidade Federal Fluminense (UFF), Instituto de Biologia Marinha, Outeiro São João Batista, s/nº, Niterói, Rio de Janeiro, CEP 24001-970, RJ, Brazil 3 Universidade do Estado do Rio de Janeiro (UERJ). Rua São Francisco Xavier, 524, Maracanã, Rio de Janeiro, CEP 20550-900, RJ, Brazil 4 DiSTeVA, Università degli Studi di Urbino “Carlo Bo”, Campus Scientifico Enrico Mattei. Località Crocicchia, 61029 Urbino, Italy 5 Laboratório de Palinofácies e Fácies Orgânicas (LAFO), Universidade Federal do Rio de Janeiro (UFRJ). Avenida Pedro Calmon, 550, Cidade Universitária, Rio de Janeiro, CEP 21941-901, RJ, Brazil 6 Laboratório de Ecologia Bêntica, Universidade Federal do Estado do Rio de Janeiro – UNIRIO. Avenida Pasteur 458, Urca, Rio de Janeiro, CEP 22290-240, RJ, Brazil * Corresponding author. E-mail: [email protected] Abstract: Itaipu Lagoon is located near the mouth of There are many advantages of applying foraminifera Guanabara Bay and has great importance for recreation to environmental monitoring when compared with to the city of Niterói, Rio de Janeiro state, Brazil. -
New Insights Into the Behavioural Ecology of Intertidal Foraminifera
Journal of Foraminiferal Research, v. 45, no. 4, p. 390–401, October 2015 THE DEVIL LIES IN DETAILS: NEW INSIGHTS INTO THE BEHAVIOURAL ECOLOGY OF INTERTIDAL FORAMINIFERA LAURENT SEURONT1,3 AND VINCENT M. P. BOUCHET2 ABSTRACT To validate in-situ observations, living foraminifera have The motion behaviour of three species of intertidal been used in the laboratory for nearly a century (e.g., Myers, foraminifera, Ammonia tepida, Cribroelphidium excavatum 1935; Le Calvez, 1938; Jepps, 1942; Arnold, 1953). In contrast, and Haynesina germanica, was investigated continuously in the the understanding of the behavioural ecology of foraminifera laboratory. We first infer the presence of geotactic and is still in its infancy, despite a fair amount of work related to phototactic responses. Significant geotactic responses were their vertical and horizontal rates of movement (Arnold, 1953, observed for all three species; A. tepida was found to be 1974; Zmiri et al., 1974; Severin & Erskian, 1981; Severin negatively geotactic while C. excavatum and H. germanica et al., 1982; Severin, 1987; Kitazato, 1988; Wetmore, 1988; showed positive geotaxis. In contrast, no response to light was Weinberg, 1991; Anderson et al., 1991; Bornmalm et al., 1997; ever observed. The detailed nature of motility, investigated in Manley & Shaw, 1997; Bernhard, 2000; Gross, 2000; Khare & terms of both geometric and stochastic complexity of their Nigam, 2000). motion behaviour, was consistently characterised by a strong Negative geotaxis is by far the most widely reported inter-specific, inter-individual and intra-individual variability. behavioural property among foraminifera (Murray, 1963, Specifically, A. tepida and H. germanica were characterised by 1979, 1991; Richter, 1964; Lee et al., 1969; Moodley, 1990), an intensive search behaviour (they explore their environment which has been routinely used to separate them from the slowly with straighter trajectories), while C. -
Checklist, Assemblage Composition, and Biogeographic Assessment of Recent Benthic Foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes
Zootaxa 4731 (2): 151–192 ISSN 1175-5326 (print edition) https://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2020 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4731.2.1 http://zoobank.org/urn:lsid:zoobank.org:pub:560FF002-DB8B-405A-8767-09628AEDBF04 Checklist, assemblage composition, and biogeographic assessment of Recent benthic foraminifera (Protista, Rhizaria) from São Vincente, Cape Verdes JOACHIM SCHÖNFELD1,3 & JULIA LÜBBERS2 1GEOMAR Helmholtz-Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany 2Institute of Geosciences, Christian-Albrechts-University, Ludewig-Meyn-Straße 14, 24118 Kiel, Germany 3Corresponding author. E-mail: [email protected] Abstract We describe for the first time subtropical intertidal foraminiferal assemblages from beach sands on São Vincente, Cape Verdes. Sixty-five benthic foraminiferal species were recognised, representing 47 genera, 31 families, and 8 superfamilies. Endemic species were not recognised. The new checklist largely extends an earlier record of nine benthic foraminiferal species from fossil carbonate sands on the island. Bolivina striatula, Rosalina vilardeboana and Millettiana milletti dominated the living (rose Bengal stained) fauna, while Elphidium crispum, Amphistegina gibbosa, Quinqueloculina seminulum, Ammonia tepida, Triloculina rotunda and Glabratella patelliformis dominated the dead assemblages. The living fauna lacks species typical for coarse-grained substrates. Instead, there were species that had a planktonic stage in their life cycle. The living fauna therefore received a substantial contribution of floating species and propagules that may have endured a long transport by surface ocean currents. The dead assemblages largely differed from the living fauna and contained redeposited tests deriving from a rhodolith-mollusc carbonate facies at <20 m water depth. -
The Metabolic Response of Ubiquitous Benthic Foraminifera (Ammonia Tepida)
RESEARCH ARTICLE Surviving anoxia in marine sediments: The metabolic response of ubiquitous benthic foraminifera (Ammonia tepida) Charlotte LeKieffre1*, Jorge E. Spangenberg2, Guillaume Mabilleau3, SteÂphane Escrig1, Anders Meibom1,4*, Emmanuelle Geslin5* 1 Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique FeÂdeÂrale de Lausanne (EPFL), Lausanne, Switzerland, 2 Stable Isotope and Organic Geochemistry Laboratories, Institute of Earth Surface Dynamics (IDYST), University of Lausanne, a1111111111 Lausanne, Switzerland, 3 Service commun d'imageries et d'analyses microscopiques (SCIAM), Institut de a1111111111 Biologie en SanteÂ, University of Angers, Angers, France, 4 Center for Advanced Surface Analysis, Institute of a1111111111 Earth Sciences, University of Lausanne, Lausanne, Switzerland, 5 UMR CNRS 6112 - LPG-BIAF, University a1111111111 of Angers, Angers, France a1111111111 * [email protected] (CL); [email protected] (AM); [email protected] (EG) Abstract OPEN ACCESS High input of organic carbon and/or slowly renewing bottom waters frequently create periods Citation: LeKieffre C, Spangenberg JE, Mabilleau G, Escrig S, Meibom A, Geslin E (2017) Surviving with low dissolved oxygen concentrations on continental shelves and in coastal areas; such anoxia in marine sediments: The metabolic events can have strong impacts on benthic ecosystems. Among the meiofauna living in these response of ubiquitous benthic foraminifera environments, benthic foraminifera are often the most tolerant to low oxygen levels. Indeed, (Ammonia tepida). PLoS ONE 12(5): e0177604. https://doi.org/10.1371/journal.pone.0177604 some species are able to survive complete anoxia for weeks to months. One known mecha- nism for this, observed in several species, is denitrification. For other species, a state of Editor: Bo Thamdrup, University of Southern Denmark, DENMARK highly reduced metabolism, essentially a state of dormancy, has been proposed but never demonstrated. -
Ciliate Diversity, Community Structure, and Novel Taxa in Lakes of the Mcmurdo Dry Valleys, Antarctica
Reference: Biol. Bull. 227: 175–190. (October 2014) © 2014 Marine Biological Laboratory Ciliate Diversity, Community Structure, and Novel Taxa in Lakes of the McMurdo Dry Valleys, Antarctica YUAN XU1,*†, TRISTA VICK-MAJORS2, RACHAEL MORGAN-KISS3, JOHN C. PRISCU2, AND LINDA AMARAL-ZETTLER4,5,* 1Laboratory of Protozoology, Institute of Evolution & Marine Biodiversity, Ocean University of China, Qingdao 266003, China; 2Montana State University, Department of Land Resources and Environmental Sciences, 334 Leon Johnson Hall, Bozeman, Montana 59717; 3Department of Microbiology, Miami University, Oxford, Ohio 45056; 4The Josephine Bay Paul Center for Comparative Molecular Biology and Evolution, Marine Biological Laboratory, Woods Hole, Massachusetts 02543; and 5Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, Rhode Island 02912 Abstract. We report an in-depth survey of next-genera- trends in dissolved oxygen concentration and salinity may tion DNA sequencing of ciliate diversity and community play a critical role in structuring ciliate communities. A structure in two permanently ice-covered McMurdo Dry PCR-based strategy capitalizing on divergent eukaryotic V9 Valley lakes during the austral summer and autumn (No- hypervariable region ribosomal RNA gene targets unveiled vember 2007 and March 2008). We tested hypotheses on the two new genera in these lakes. A novel taxon belonging to relationship between species richness and environmental an unknown class most closely related to Cryptocaryon conditions -
Protist Phylogeny and the High-Level Classification of Protozoa
Europ. J. Protistol. 39, 338–348 (2003) © Urban & Fischer Verlag http://www.urbanfischer.de/journals/ejp Protist phylogeny and the high-level classification of Protozoa Thomas Cavalier-Smith Department of Zoology, University of Oxford, South Parks Road, Oxford, OX1 3PS, UK; E-mail: [email protected] Received 1 September 2003; 29 September 2003. Accepted: 29 September 2003 Protist large-scale phylogeny is briefly reviewed and a revised higher classification of the kingdom Pro- tozoa into 11 phyla presented. Complementary gene fusions reveal a fundamental bifurcation among eu- karyotes between two major clades: the ancestrally uniciliate (often unicentriolar) unikonts and the an- cestrally biciliate bikonts, which undergo ciliary transformation by converting a younger anterior cilium into a dissimilar older posterior cilium. Unikonts comprise the ancestrally unikont protozoan phylum Amoebozoa and the opisthokonts (kingdom Animalia, phylum Choanozoa, their sisters or ancestors; and kingdom Fungi). They share a derived triple-gene fusion, absent from bikonts. Bikonts contrastingly share a derived gene fusion between dihydrofolate reductase and thymidylate synthase and include plants and all other protists, comprising the protozoan infrakingdoms Rhizaria [phyla Cercozoa and Re- taria (Radiozoa, Foraminifera)] and Excavata (phyla Loukozoa, Metamonada, Euglenozoa, Percolozoa), plus the kingdom Plantae [Viridaeplantae, Rhodophyta (sisters); Glaucophyta], the chromalveolate clade, and the protozoan phylum Apusozoa (Thecomonadea, Diphylleida). Chromalveolates comprise kingdom Chromista (Cryptista, Heterokonta, Haptophyta) and the protozoan infrakingdom Alveolata [phyla Cilio- phora and Miozoa (= Protalveolata, Dinozoa, Apicomplexa)], which diverged from a common ancestor that enslaved a red alga and evolved novel plastid protein-targeting machinery via the host rough ER and the enslaved algal plasma membrane (periplastid membrane). -
A Guide to 1.000 Foraminifera from Southwestern Pacific New Caledonia
Jean-Pierre Debenay A Guide to 1,000 Foraminifera from Southwestern Pacific New Caledonia PUBLICATIONS SCIENTIFIQUES DU MUSÉUM Debenay-1 7/01/13 12:12 Page 1 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Debenay-1 7/01/13 12:12 Page 2 Debenay-1 7/01/13 12:12 Page 3 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Jean-Pierre Debenay IRD Éditions Institut de recherche pour le développement Marseille Publications Scientifiques du Muséum Muséum national d’Histoire naturelle Paris 2012 Debenay-1 11/01/13 18:14 Page 4 Photos de couverture / Cover photographs p. 1 – © J.-P. Debenay : les foraminifères : une biodiversité aux formes spectaculaires / Foraminifera: a high biodiversity with a spectacular variety of forms p. 4 – © IRD/P. Laboute : îlôt Gi en Nouvelle-Calédonie / Island Gi in New Caledonia Sauf mention particulière, les photos de cet ouvrage sont de l'auteur / Except particular mention, the photos of this book are of the author Préparation éditoriale / Copy-editing Yolande Cavallazzi Maquette intérieure et mise en page / Design and page layout Aline Lugand – Gris Souris Maquette de couverture / Cover design Michelle Saint-Léger Coordination, fabrication / Production coordination Catherine Plasse La loi du 1er juillet 1992 (code de la propriété intellectuelle, première partie) n'autorisant, aux termes des alinéas 2 et 3 de l'article L. 122-5, d'une part, que les « copies ou reproductions strictement réservées à l'usage privé du copiste et non destinées à une utilisation collective » et, d'autre part, que les analyses et les courtes citations dans un but d'exemple et d'illustration, « toute représentation ou reproduction intégrale ou partielle, faite sans le consentement de l'auteur ou de ses ayants droit ou ayants cause, est illicite » (alinéa 1er de l'article L. -
23.3 Groups of Protists
Chapter 23 | Protists 639 cysts that are a protective, resting stage. Depending on habitat of the species, the cysts may be particularly resistant to temperature extremes, desiccation, or low pH. This strategy allows certain protists to “wait out” stressors until their environment becomes more favorable for survival or until they are carried (such as by wind, water, or transport on a larger organism) to a different environment, because cysts exhibit virtually no cellular metabolism. Protist life cycles range from simple to extremely elaborate. Certain parasitic protists have complicated life cycles and must infect different host species at different developmental stages to complete their life cycle. Some protists are unicellular in the haploid form and multicellular in the diploid form, a strategy employed by animals. Other protists have multicellular stages in both haploid and diploid forms, a strategy called alternation of generations, analogous to that used by plants. Habitats Nearly all protists exist in some type of aquatic environment, including freshwater and marine environments, damp soil, and even snow. Several protist species are parasites that infect animals or plants. A few protist species live on dead organisms or their wastes, and contribute to their decay. 23.3 | Groups of Protists By the end of this section, you will be able to do the following: • Describe representative protist organisms from each of the six presently recognized supergroups of eukaryotes • Identify the evolutionary relationships of plants, animals, and fungi within the six presently recognized supergroups of eukaryotes • Identify defining features of protists in each of the six supergroups of eukaryotes. In the span of several decades, the Kingdom Protista has been disassembled because sequence analyses have revealed new genetic (and therefore evolutionary) relationships among these eukaryotes. -
Phylogenomics Supports the Monophyly of the Cercozoa T ⁎ Nicholas A.T
Molecular Phylogenetics and Evolution 130 (2019) 416–423 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Phylogenomics supports the monophyly of the Cercozoa T ⁎ Nicholas A.T. Irwina, , Denis V. Tikhonenkova,b, Elisabeth Hehenbergera,1, Alexander P. Mylnikovb, Fabien Burkia,2, Patrick J. Keelinga a Department of Botany, University of British Columbia, Vancouver V6T 1Z4, British Columbia, Canada b Institute for Biology of Inland Waters, Russian Academy of Sciences, Borok 152742, Russia ARTICLE INFO ABSTRACT Keywords: The phylum Cercozoa consists of a diverse assemblage of amoeboid and flagellated protists that forms a major Cercozoa component of the supergroup, Rhizaria. However, despite its size and ubiquity, the phylogeny of the Cercozoa Rhizaria remains unclear as morphological variability between cercozoan species and ambiguity in molecular analyses, Phylogeny including phylogenomic approaches, have produced ambiguous results and raised doubts about the monophyly Phylogenomics of the group. Here we sought to resolve these ambiguities using a 161-gene phylogenetic dataset with data from Single-cell transcriptomics newly available genomes and deeply sequenced transcriptomes, including three new transcriptomes from Aurigamonas solis, Abollifer prolabens, and a novel species, Lapot gusevi n. gen. n. sp. Our phylogenomic analysis strongly supported a monophyletic Cercozoa, and approximately-unbiased tests rejected the paraphyletic topologies observed in previous studies. The transcriptome of L. gusevi represents the first transcriptomic data from the large and recently characterized Aquavolonidae-Treumulida-'Novel Clade 12′ group, and phyloge- nomics supported its position as sister to the cercozoan subphylum, Endomyxa. These results provide insights into the phylogeny of the Cercozoa and the Rhizaria as a whole. -
New Phylogenomic Analysis of the Enigmatic Phylum Telonemia Further Resolves the Eukaryote Tree of Life
bioRxiv preprint doi: https://doi.org/10.1101/403329; this version posted August 30, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. New phylogenomic analysis of the enigmatic phylum Telonemia further resolves the eukaryote tree of life Jürgen F. H. Strassert1, Mahwash Jamy1, Alexander P. Mylnikov2, Denis V. Tikhonenkov2, Fabien Burki1,* 1Department of Organismal Biology, Program in Systematic Biology, Uppsala University, Uppsala, Sweden 2Institute for Biology of Inland Waters, Russian Academy of Sciences, Borok, Yaroslavl Region, Russia *Corresponding author: E-mail: [email protected] Keywords: TSAR, Telonemia, phylogenomics, eukaryotes, tree of life, protists bioRxiv preprint doi: https://doi.org/10.1101/403329; this version posted August 30, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Abstract The broad-scale tree of eukaryotes is constantly improving, but the evolutionary origin of several major groups remains unknown. Resolving the phylogenetic position of these ‘orphan’ groups is important, especially those that originated early in evolution, because they represent missing evolutionary links between established groups. Telonemia is one such orphan taxon for which little is known. The group is composed of molecularly diverse biflagellated protists, often prevalent although not abundant in aquatic environments. -
Anaerobic Metabolism of Foraminifera Thriving Below the Seafloor 2 3 Authors: William D
bioRxiv preprint doi: https://doi.org/10.1101/2020.03.26.009324; this version posted March 27, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Anaerobic metabolism of Foraminifera thriving below the seafloor 2 3 Authors: William D. Orsi1,2*, Raphaël Morard4, Aurele Vuillemin1, Michael Eitel1, Gert Wörheide1,2,3, 4 Jana Milucka5, Michal Kucera4 5 Affiliations: 6 1. Department of Earth and Environmental Sciences, Paleontology & Geobiology, Ludwig-Maximilians- 7 Universität München, 80333 Munich, Germany. 8 2. GeoBio-CenterLMU, Ludwig-Maximilians-Universität München, 80333 Munich, Germany 9 3. SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, 80333 Munich, Germany 10 4. MARUM – Center for Marine Environmental Sciences, University of Bremen, Germany 11 5. Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Bremen, Germany 12 13 *To whom correspondence should be addressed: [email protected] 14 15 Abstract: Foraminifera are single-celled eukaryotes (protists) of large ecological importance, as well as 16 environmental and paleoenvironmental indicators and biostratigraphic tools. In addition, they are capable 17 of surviving in anoxic marine environments where they represent a major component of the benthic 18 community. However, the cellular adaptations of Foraminifera to the anoxic environment remain poorly 19 constrained. We sampled an oxic-anoxic transition zone in marine sediments from the Namibian shelf, 20 where the genera Bolivina and Stainforthia dominated the Foraminifera community, and use 21 metatranscriptomics to characterize Foraminifera metabolism across the different geochemical 22 conditions.